Modeling for Inter-Basin Groundwater Transfer Identification Between Middle Abay River Basin and Upper Awash River Basin

Total Page:16

File Type:pdf, Size:1020Kb

Modeling for Inter-Basin Groundwater Transfer Identification Between Middle Abay River Basin and Upper Awash River Basin Modeling for Inter-Basin Groundwater Transfer Identification between Middle Abay River Basin and Upper Awash River Basin By: Dure Mulatu Addis Ababa University Addis Ababa, Ethiopia June, 2017 Addis Ababa University Addis Ababa Institute of Technology School of Graduate Studies School of Civil and Environmental Engineering Modeling for Inter-Basin Groundwater Transfer Identification between Middle Abay River Basin and Upper Awash River Basin By: Dure Mulatu A thesis submitted to the School of Graduate Studies of Addis Ababa University in Partial fulfillment of the Degree of Master of Science in Hydraulic Engineering. Advisor: Dr - Ing Mebruk Mohammed June, 2017 Addis Ababa University Addis Ababa Institute of Technology School of Graduate Studies School of Civil and Environmental Engineering Modeling for Inter-Basin Groundwater Transfer Identification between Middle Abay River Basin and Upper Awash River Basin A thesis submitted to the School of Graduate Studies of Addis Ababa University in Partial fulfillment of the Degree of Master of Science in Hydraulic Engineering. By: Dure Mulatu Approval by Board of Examiners Dr. Ing Mebruk Mohammed ------------------------------ Advisor Signature Dr. Agizew Nigussie ------------------------------- Internal Examiner Signature Dr. Belete Birhanu ------------------------------- External Examiner Signature Dedication To my mother Kibe Balcha whom I love very much Abstract Groundwater flow models are important for the identification of inter-basin groundwater transfer between adjacent basins. Numerical groundwater model, TAGSAC has been used to study the inter-basin groundwater transfer (IBGWT) between middle Abay River basin and upper Awash River basin. Three steady state groundwater flow models (for middle Abay River basin, upper Awash River basin and for the two combined basins) were first created and calibrated for the inventoried wells. The first two models were created by considering the surface water divide between the two basins as a no flow boundary. The third model avoids the surface water divide which justifies IBGWT. The calibration target for this study was the hydraulic head; hydraulic conductivity and surface recharge were used as calibration parameters. The goodness of fit indicators (GoFIs) that was obtained for the third model was better than the other two models. This indicates the evidence of IBGWT between the two basins; i.e. groundwater flows from middle Abay River basin to Upper Awash River basin and from Upper Awash River basin to middle Abay River basin. In addition, the groundwater head distribution for third model showed that the groundwater divide and surface water divide were not coincident. And groundwater is easily accessed within a shallower depth in the Upper Awash River basin compared to the middle Abay River basin. Keywords: Inter-Basin Groundwater Transfer, Numerical Groundwater Modeling, TAGSAC, Middle Abay River Basin, Upper Awash River Basin, Ethiopia Addis Ababa Institute of Technology | I Acknowledgments First of all, I would like to thank the almighty God for providing His grace, love and support throughout this journey. I have the greatest appreciation for my advisor, Dr. Ing Mebruk Mohammed, who invested his time, knowledge and energy throughout the study. His guidance, dedication and encouragements throughout the study were amazing. I am very grateful to the Ethiopian Road Authority (ERA) scholarship for making it possible for me to study in Addis Ababa institute of Technology. I also thank organizations: Water Works Design and Supervision Enterprise and Ministry of Water Resources for providing the required secondary data. Lastly, I would like to thank my family and friends for their constant support and encouragements. Addis Ababa Institute of Technology | II Table of Contents Abstract ....................................................................................................................................... I Acknowledgments..................................................................................................................... II List of Figures ........................................................................................................................... V List of Tables ........................................................................................................................... VI List of Acronyms ................................................................................................................... VII 1 Introduction ........................................................................................................................ 1 1.1 Statement of the problem ............................................................................................ 2 1.2 Objective ..................................................................................................................... 2 1.3 Structure of the thesis .................................................................................................. 3 2 Literature Review ............................................................................................................... 4 2.1 Inter-basin Flow .......................................................................................................... 4 2.2 Previous Studies .......................................................................................................... 4 2.3 Groundwater ................................................................................................................ 7 2.3.1 Groundwater Potential ......................................................................................... 7 2.3.2 Groundwater Recharge ........................................................................................ 7 2.3.3 Fractured Media ................................................................................................... 9 2.3.4 Groundwater Modeling ...................................................................................... 10 2.3.5 Groundwater Flow Equation .............................................................................. 12 2.3.6 Boundary Conditions ......................................................................................... 15 3 Materials and Methods ..................................................................................................... 18 3.1 Description of the Study Area ................................................................................... 18 3.1.1 Location of the Study Area ................................................................................ 18 3.1.2 Hydrometeorology ............................................................................................. 19 3.2 Data processing ......................................................................................................... 19 3.3 Modeling for inter-basin groundwater transfer ......................................................... 19 3.4 Data Collection and Analysis .................................................................................... 21 Addis Ababa Institute of Technology | III 3.4.1 Meteorology ....................................................................................................... 22 3.4.2 Topography ........................................................................................................ 26 3.4.3 Well and spring inventory .................................................................................. 26 3.4.4 Geology .............................................................................................................. 27 3.5 Conceptual Model ..................................................................................................... 29 3.6 Groundwater Modeling ............................................................................................. 30 3.6.1 Model selection .................................................................................................. 30 3.6.2 Discretization ..................................................................................................... 31 3.6.3 Boundary Conditions ......................................................................................... 32 3.6.4 Recharge Boundary ............................................................................................ 32 4 Result and Discussions ..................................................................................................... 34 4.1 Model Discretization ................................................................................................. 34 4.2 Model calibration results ........................................................................................... 36 4.3 Hydrogeology ............................................................................................................ 43 4.4 Groundwater flow direction ...................................................................................... 46 4.5 Groundwater Accessibility ........................................................................................ 50 5 Conclusion and Recommendation .................................................................................... 52 5.1 Conclusion ................................................................................................................. 52 5.2 Recommendation ....................................................................................................... 53 6 References .......................................................................................................................
Recommended publications
  • Local History of Ethiopia Ma - Mezzo © Bernhard Lindahl (2008)
    Local History of Ethiopia Ma - Mezzo © Bernhard Lindahl (2008) ma, maa (O) why? HES37 Ma 1258'/3813' 2093 m, near Deresge 12/38 [Gz] HES37 Ma Abo (church) 1259'/3812' 2549 m 12/38 [Gz] JEH61 Maabai (plain) 12/40 [WO] HEM61 Maaga (Maago), see Mahago HEU35 Maago 2354 m 12/39 [LM WO] HEU71 Maajeraro (Ma'ajeraro) 1320'/3931' 2345 m, 13/39 [Gz] south of Mekele -- Maale language, an Omotic language spoken in the Bako-Gazer district -- Maale people, living at some distance to the north-west of the Konso HCC.. Maale (area), east of Jinka 05/36 [x] ?? Maana, east of Ankar in the north-west 12/37? [n] JEJ40 Maandita (area) 12/41 [WO] HFF31 Maaquddi, see Meakudi maar (T) honey HFC45 Maar (Amba Maar) 1401'/3706' 1151 m 14/37 [Gz] HEU62 Maara 1314'/3935' 1940 m 13/39 [Gu Gz] JEJ42 Maaru (area) 12/41 [WO] maass..: masara (O) castle, temple JEJ52 Maassarra (area) 12/41 [WO] Ma.., see also Me.. -- Mabaan (Burun), name of a small ethnic group, numbering 3,026 at one census, but about 23 only according to the 1994 census maber (Gurage) monthly Christian gathering where there is an orthodox church HET52 Maber 1312'/3838' 1996 m 13/38 [WO Gz] mabera: mabara (O) religious organization of a group of men or women JEC50 Mabera (area), cf Mebera 11/41 [WO] mabil: mebil (mäbil) (A) food, eatables -- Mabil, Mavil, name of a Mecha Oromo tribe HDR42 Mabil, see Koli, cf Mebel JEP96 Mabra 1330'/4116' 126 m, 13/41 [WO Gz] near the border of Eritrea, cf Mebera HEU91 Macalle, see Mekele JDK54 Macanis, see Makanissa HDM12 Macaniso, see Makaniso HES69 Macanna, see Makanna, and also Mekane Birhan HFF64 Macargot, see Makargot JER02 Macarra, see Makarra HES50 Macatat, see Makatat HDH78 Maccanissa, see Makanisa HDE04 Macchi, se Meki HFF02 Macden, see May Mekden (with sub-post office) macha (O) 1.
    [Show full text]
  • Revision of the Genus Ficus L. (Moraceae) in Ethiopia (Primitiae Africanae Xi)
    582.635.34(63) MEDEDELINGEN LANDBOUWHOGESCHOOL WAGENINGEN • NEDERLAND • 79-3 (1979) REVISION OF THE GENUS FICUS L. (MORACEAE) IN ETHIOPIA (PRIMITIAE AFRICANAE XI) G. AWEKE Laboratory of Plant Taxonomy and Plant Geography, Agricultural University, Wageningen, The Netherlands Received l-IX-1978 Date of publication 27-4-1979 H. VEENMAN & ZONEN B.V.-WAGENINGEN-1979 BIBLIOTHEEK T)V'. CONTENTS page INTRODUCTION 1 General remarks 1 Uses, actual andpossible , of Ficus 1 Method andarrangemen t ofth e revision 2 FICUS L 4 KEY TOTH E FICUS SPECIES IN ETHIOPIA 6 ALPHABETICAL TREATMENT OFETHIOPIA N FICUS SPECIES 9 Ficus abutilifolia (MIQUEL)MIQUEL 9 capreaefolia DELILE 11 carica LINNAEUS 15 dicranostyla MILDBRAED ' 18 exasperata VAHL 21 glumosu DELILE 25 gnaphalocarpa (MIQUEL) A. RICHARD 29 hochstetteri (MIQUEL) A. RICHARD 33 lutea VAHL 37 mallotocarpa WARBURG 41 ovata VAHL 45 palmata FORSKÀL 48 platyphylla DELILE 54 populifolia VAHL 56 ruspolii WARBURG 60 salicifolia VAHL 62 sur FORSKÂL 66 sycomorus LINNAEUS 72 thonningi BLUME 78 vallis-choudae DELILE 84 vasta FORSKÂL 88 vogelii (MIQ.) MIQ 93 SOME NOTES ON FIGS AND FIG-WASPS IN ETHIOPIA 97 Infrageneric classification of Hewsaccordin gt o HUTCHINSON, related to wasp-genera ... 99 Fig-wasp species collected from Ethiopian figs (Agaonid associations known from extra- limitalsample sadde d inparentheses ) 99 REJECTED NAMES ORTAX A 103 SUMMARY 105 ACKNOWLEDGEMENTS 106 LITERATURE REFERENCES 108 INDEX 112 INTRODUCTION GENERAL REMARKS Ethiopia is as regards its wild and cultivated plants, a recognized centre of genetically important taxa. Among its economic resources, agriculture takes first place. For this reason, a thorough knowledge of the Ethiopian plant cover - its constituent taxa, their morphology, life-cycle, cytogenetics etc.
    [Show full text]
  • The Grand Ethiopian Renaissance Dam and Ethiopia's Succession in Hydro-Legal Prominence
    The Grand Ethiopian Renaissance Dam and Ethiopia’s Succession in Hydro-legal Prominence: A Script in Legal History of Diplomatic Confront (1957-2013) Tadesse Kassa Woldetsadik . Abstract This article argues that within the system of international law, while Ethiopia’s equitable right of access to resources of the Nile is recognized as a matter of settled principle, the law’s actual working is a coefficient of prior hydraulic measures adopted on the ground rather than mere articulation of legal norms, diplomatic civility or altercations. I also submit that the system of international law still remains vital in resolving transboundary water issues, and yet, the mechanics of law could not function optimally outside of power politic, diplomatic dexterity and sincere commitment to the fundamental values it upholds. In this light, and against a backdrop of Ethiopia’s relegated position in the second half of the twentieth century, the paper concludes that today the country’s relative renaissance in the Nile legal politics - which for the first time captured serious downstream interest in riparian negotiations - is attributed not to a change in the pertinence of the norms of international law nor to any altruistic revision of positions in the lower reaches of the river, but rather to its belated awakening in pursuing the Grand Ethiopian Renaissance Dam (GERD) as a national project of multifarious impact. Key terms The Grand Ethiopian Renaissance Dam, Nile water resources development, Nile, legal diplomacy, Ethiopia, Egypt, Sudan. DOI http://dx.doi.org/10.4314/mlr.v9i2.5 ___________ Introduction In an article published in Mizan 8(2) focusing on the legal history and diplomatic minutiae of the first half of the twentieth century (1902-1956), it was argued that the Anglo-Ethiopian Treaty of 1902 on the Blue Nile and the stream of negotiations conducted in the immediate aftermath in relation to the Lake Tana .
    [Show full text]
  • List of Rivers of Ethiopia
    Sl. No Name Location (Flowing into) Location (Lake) 1 Adar River (South Sudan) The Mediterranean 2 Akaki River Endorheic basins Afar Depression 3 Akobo River The Mediterranean 4 Ala River Endorheic basins Afar Depression 5 Alero River (or Alwero River) The Mediterranean 6 Angereb River (or Greater Angereb River) The Mediterranean 7 Ataba River The Mediterranean 8 Ataye River Endorheic basins Afar Depression 9 Atbarah River The Mediterranean 10 Awash River Endorheic basins Afar Depression 11 Balagas River The Mediterranean 12 Baro River The Mediterranean 13 Bashilo River The Mediterranean 14 Beles River The Mediterranean 15 Bilate River Endorheic basins Lake Abaya 16 Birbir River The Mediterranean 17 Blue Nile (or Abay River) The Mediterranean 18 Borkana River Endorheic basins Afar Depression 19 Checheho River The Mediterranean 20 Dabus River The Mediterranean 21 Daga River (Deqe Sonka Shet) The Mediterranean 22 Dawa River The Indian Ocean 23 Dechatu River Endorheic basins Afar Depression 24 Dembi River The Mediterranean 25 Denchya River Endorheic basins Lake Turkana 26 Didessa River The Mediterranean 27 Dinder River The Mediterranean 28 Dipa River The Mediterranean 29 Dungeta River The Indian Ocean 30 Durkham River Endorheic basins Afar Depression 31 Erer River The Indian Ocean 32 Fafen River (only reaches the Shebelle in times of flood) The Indian Ocean 33 Galetti River The Indian Ocean 34 Ganale Dorya River The Indian Ocean 35 Gebba River The Mediterranean 36 Germama River (or Kasam River) Endorheic basins Afar Depression 37 Gibe River
    [Show full text]
  • Ethiopia): Findings from a DEM Michal Kusák1,*, Vít Vilímek2, Jozef Minár3
    Original Article 129 Influence of neotectonics on land surface evolution in the upper part of the Blue Nile Basin (Ethiopia): findings from a DEM Michal Kusák1,*, Vít Vilímek2, Jozef Minár3 1 Institute of Rock Structure and Mechanics of the Czech Academy of Sciences, Czech Republic 2 Charles University, Faculty of Science, Department of Physical Geography and Geoecology, Czech Republic 3 Comenius University in Bratislava, Faculty of Natural Sciences, Department of Physical Geography and Geoecology, Slovak Republic * Corresponding author: [email protected] ABSTRACT The morphometric analysis of lineaments, valleys and signs of erosion taken from a digital elevation model (DEM) made it possible to not only confirm most of the conclusions of the morphotectonic development of the Blue Nile Basin from the previously pub- lished results of structural, petrological, tectonic and geochronological analyses, but also to expand our knowledge by applying several new hypotheses. The relative age of the morpholineaments of particular directions was estimated from the character of topographic profiles. Faults, lineaments and valleys are predominantly oriented in a direction compatible to the published concepts of the tectonic development of the area. Overall, the most abundant NE-SW and NNE-SSW lines reflect a change of extension from a NW-SE to WNW-ESE direction during the Pliocene, in relation to the creation and development of the Main Ethiopian Rift (MER). This is confirmed by a more developed character of the valleys and less pronounced erosion activity of the NE-SW oriented valleys contrary to the deeper narrower NNE-SSW valleys characterised by downward and headward erosion in the second direction.
    [Show full text]
  • United States Cooperative Progra 1961 Annual Report
    ETOPIA -UNITED STATES COOPERATIVE PROGRA FOR THE STUDY OF WATER RESOURCES In Collaboration With United States ited States Department of State Int'l. Cooperation Admna. Department of the Interior Bureau of ReclamAtion Imperial Ethiopian Government Ministry of Public Works and Communications Water Resources Department 1961 ANNUAL REPORT OF THE BUREAU OF RECLAMATION ON TI[E BLUE NILE RIVER BASIN INVESTIGATIONS Washington, D. C. December 31, 1961 .I. D" Reference Cen'Te- Room 1656 NS UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF RECLAMATION WASHINGTON 25, D. C. IN REPLY REFER TO! 220 December 31, 1961 Mr. Allen Loren, Director USAID to Ethiopia c/o American Embassy Addis Ababa, Ethiopia Dear Mr. Loren: Under the terms of the Agreement, dated August 9, 1957, between the Department of the Interior and the Department of State, providing for Water Resources Investigations in the Blue Nile River Basin, Ethiopia, an annual report is required. It is a pleasure to submit herewith the annual report for the calendar year 1961. This is the fourth such report, the project being in the fifth ot six years as now programed. Sincerely yours, o er Co s •w-.VQ ..',t. ~Vy Finchaa Falls One of the more promising future developments is associated with the use of Chomen Swamp, above the falls, for storage, and the irrigation of land in the lower valley, coupled with a power installation below the falls. 1961 ANNUAL REPORT BLUE NILE RIVER BASIN INVESTIGATIONS CONTE NTS Photo of Finchaa Falls Frontispiece I. Introduction....................................... ...I. .. Fig. 1 - Organization for Project Operations 1962 II. Conduct of Operations ...................................
    [Show full text]
  • Ethiopia and the Nile Dilemmas of National and Regional Hydropolitics
    Research Collection Doctoral Thesis Ethiopia and the Nile Dilemmas of national and regional hydropolitics Author(s): Arsano, Yacob Publication Date: 2007 Permanent Link: https://doi.org/10.3929/ethz-a-005380361 Rights / License: In Copyright - Non-Commercial Use Permitted This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Yacob Arsano Ethiopia and the Nile Dilemmas of National and Regional Hydropolitics © 2007, ETH Zurich and Yacob Arsano Center for Security Studies, Swiss Federal Institute of Technology, Zurich ETH Zentrum SEI, Seilergraben 49, CH-8092-Zurich, Switzerland. Tel. ++41 (0)44 632 40 25 Fax ++41 (0)44 632 19 41 www.css.ethz.ch Author contact Yacob Arsano, Addis Ababa University, Department of Political Sciences and International Relations, Email: [email protected] Fulltext online available at www.isn.ethz.ch All rights reserved. No part of this publication may be used or reproduced in any manner whatsoever without the prior written permission of the author except in the case of brief quotations embodied in critical articles and reviews. Cover-Photo Tis Isat Falls / Blue Nile Falls by Torleif Svensson Layout and graphics Fabian Furter Fonts Adobe Caslon Pro News Gothic Std. (Cover) ISBN 3-905696-14-2 Ethiopia and the Nile Dilemmas of National and Regional Hydropolitics Thesis presented to the Faculty of Arts of the University of Zurich for the degree of Doctor of Philosophy by Yacob Arsano of Ethiopia Accepted in the summer semester on the recommendation of Prof. Dr. Andreas Wenger and Prof.
    [Show full text]
  • Ethiopian Environment and Forest Research Institute
    የኢትዮጵያ የአካባቢና የደን ምርምር ኢንስቲትዩት ETHIOPIAN ENVIRONMNET AND FOREST RESEARCH INSTITUTE Forest and Environment Research: Technologies and Information Edited by: Mehari Alebachew Getachew Desalegn Wubalem Tadesse Agena Anjulo Fassil Kebede i ETHIOPIAN ENVIRONMENT AND FOREST RESEARCH INSTITUTE Forest and Environment Research: Technologies and Information Edited by: Mehari Alebachew Getachew Desalegn Wubalem Tadesse Agena Anjulo Fasil Kebede PROCEEDINGS OF THE 1ST TECHNOLOGY DESSIMINATION WORKSHOP 26th - 27th November 2015 Tokuma Hotel, Adama, Ethiopia ii Table of contents WELCOME SPEECH ..................................................................................................................................... viii OPENING SPEECH .......................................................................................................................................... x PLANTATION AND AGROFORESTRY ............................................................................................................... 1 EARLY GROWTH PERFORMANCE OF JUNIPERUS PROCERA HOCHST. EX ENDL IN DEGRADED LANDS OF NORTH SHOA ................................................................................................................................................ 1 COMMUNITY ESTABLISHED EUCALYPT PLANTATIONS IN ETHIOPIA FOR DEGRADED LAND RESTORATION AND INCOME GENERATION ........................................................................................................................... 7 CHARACTERIZATION OF TRADITIONAL AGROFORESTRY PRACTICES AND SOCIOECONOMIC
    [Show full text]
  • Birds of ETHIOPIA and ERITREA
    ERITREA Massawa G Asmara ash R iv e M r a re b River r S e etit Riv Axum Ta ca zz e R i A v Mekele ngareb R e ive SIMIEN r r MTS NP Lake Afrera A tbara River Assab DANAKIL Metema DESERT Gonder Lake Ashange Doumeira nder R Di iver Lake Tana Lalibela Bahar Dar Lakes Hayk and Ardibo Aseita Beles River Dangla er Dessie iv Lake Abbe R h wetlands s a Borkena w wetlands A r Aba e y ( v B i lue Debre Markos R N il Meteka s e) J Gewani u R em wetlands Asosa b iver m a M u Rive D D ug r i er d Ri Lakes Alemaya e ve Dire Dawa Togochale s r and Adele s Fincha’a a S Ankober MT R wetlands Sululta HER Jijiga iv RC e wetlands HE r C Fafen River Dilu Meda Addis Ababa Harar Nekempte wetlands Awash Akaki wetlands Debre Zeit AWASH NP Dembidollo G Debre Zeit Lakes ib e River R Baro iv Metu er Lake Koka Degeh Bur Itang Gambela Gore ETHIOPIA Gilo R iver Metu, Gore, Lake Arakit Zwai Lake Zwai Ak ob Tepi Forests Lake Abiata Sheik Hussein o R Gok Jimma Lake Langano ive Boyo wetland r G Lake Shalla ojeb River Tepi Lake Awassa Awassa Ghinir Warder Galadi Mizan Wondo BALE MTS NP Sodo Genet Goba Harenna Kebri Dehar er Riv Forest Omo Weyb River Wa Bulcha be S Imi hab Lake Abaya ee Maji Forest lle Riv Gode Shilabo Arba Minch NECHISAR NP er OMO NP Mui Jinka Lake Chamo MAGO Kalafo NP Wadera r ve Forest Ri nale Negelle Ge Sa gan River Mustahil Kelam Arero Forest awa Yavello D Riv er Fejeje Arero Lake Chew Bahir Bogol Manyo Dolo Lake Turkana Moyale This map is not an authority on international boundaries.
    [Show full text]
  • Local History of Ethiopia Seka - Shayi © Bernhard Lindahl (2008)
    Local History of Ethiopia Seka - Shayi © Bernhard Lindahl (2008) seka (säqa, säqqa) (A) edge of cliff, crest of a hill; sekka (säkka) (A) walk along, traverse; zeka, zekat (zäkat) (A) alms among Muslims HC... Seka (Saka, Sakka, Saqqa) (historical), 07/36? [x] The so-called capital of Enarea (Enariya) was described as a town of 10,000 to 12,000 people in the 1830s. HCR41 Seka (Sek'a, Seqa, Saka, Sacca, Saca Gimma) 07/36 [Gz q WO Gu] 0736'/3644' 1828/1855 m (centre in 1964 of Chekorsa wereda, with Sunday market) HCR61 Seka (Sek'a, Seqa) 0747'/3644' 1931 m, 07/36 [Gz q] east of Agaro HDB28 Seka (Secca), see under Bedele 08/36 [+ WO] HDC03 Seka (Saca, Limmu Saca) 1841/1850 m 08/36 [Gz Te WO Gu] (Saka, Sarca, Sakwa, Haro) (with sub-post office) 08/36 [Wa Ha] 0812'/3656' 1792/1841/1850 m Within a radius of 10 km there are at km 8S Suntu (Genet, Sintu, Gennet Limmu) (village) 8SW Gabana (Gabano) (mountain) 2097 m 10NW Mile (Mole) (mountain) 1619 m HDH20 Seka, see Disi HDL31 Seka (Sek'a, Seqa) 0920'/3834' 2375 m, 09/38 [AA Gz q] north-west of Sululta HDL40 Seka (Sek'a, Seqa) 0928'/3829' 2452 m 09/38 [AA Gz q] HDL51 Seka (Sek'a, Seqa) 09/38 [AA q] JDJ23 Seka (Sek'a, Seqa) 0916'/4157' 1797 m, 09/41 [Gz q] north-east of Grawa HDK62 Seka Berke (Sek'a Berk'e, Seqa Berqe) 09/37 [AA Gz q] 0936'/3742' 2378 m, north-west of Kachisi seka ela: ela (O) deep lake or pond; clear water; eelaa (O) very heavy /load/; ela (A) well, cistern HCR41 Seka Chekorsa wereda (-1964-2004-) 07/36 [Ad] (Seka Chokorsa ..) (-1994-) is divided into 100 rural and 2 urban kebeles.
    [Show full text]
  • Local History of Ethiopia Ama - Amzanaghir © Bernhard Lindahl (2005)
    Local History of Ethiopia Ama - Amzanaghir © Bernhard Lindahl (2005) ama, hamaa (O) honeybadger, Egyptian mongoose, Herpestes ichneumon HDM13 Ama 09°11'/39°39' 1627 m 09/39 [Gz] JDH46 Ama Yusefo 09°28'/41°18' 1587 m 09/41 [Gz] HDU52c Amad Washo (recorded in 1841) 10/39 [Ha] HEC38 Amadamit, see Amedamit amado: amedu (amädu) (A) the ashes; amed washa, ash cave; ado amo (Afar) white head JEA77 Amado (area) 11/40 [WO 20] Site in the upper Mille valley south of the volcano Gura Ale and only about a couple of square kilometres in size. In October 1973 the International Afar Research Expedition with 18 people in four LandRovers visited Amado. "Amado is noteworthy for its thick, fluviatile, crystalline tuffs containing beautiful translucent fossil wood and hundreds of monkey and baboon fossils. Coppens and Guérin judged the elephants and rhinos to be between 3 and 4 million years old. Some of the associated sediments looked like hot spring deposits, and the fossil wood looked like palm." The expedition in five days collected nearly 400 fossils, a quarter of them being monkeys. [J Kalb 2001 p 100] JEC01 Amadu (Lo Ammadu, Amadoo) (plain) 10/41 [Gu WO Ha] HCJ80 Amaia (Ammaia), see Ameya HCS44 Amairaba 07°39'/37°54' 2460 m 07/37 [WO Gz] amaja: ameja, amija (A) kind of shrub or small tree, Hypericum revolutum, H. quartinianum JDJ12 Amaja (Amagia) (saddle), see under Grawa 09/41 [+ Gu] cf Ameja, Amija ?? Amajah ../.. [Pa] A Muslim settlement in eastern Shewa, near the Kessem river, "the population of which /in the 1530s/ welcomed Grañ's forces, and prayed for the latter's victory".
    [Show full text]
  • Ethiopia-Djibouti-Somaliland-5-Cover
    ©Lonely Planet Publications Pty Ltd “All you’ve got to do is decide to go and the hardest part is over. So go!” TONY WHEELER, COFOUNDER – LONELY PLANET Go further with Lonely Planet 1 Book your travels 2 Talk to other PAGE PLAN YOUR PLANNING TOOL KIT Photos, itineraries, lists and suggestions Find a fl ight travellers 2 Looking for ideas and advice on a Find the right fl ight through our YOUR TRIP to help you put together your perfect trip specifi c destination? Want to share online booking service. your experiences with the most active travel community? Then head Welcome to Ethiopia, Reserve a room to Thorn Tree, Lonely Planet’s forum, In Ethiopia, Djibouti and Visit the Lonely Planet website to book where you’ll fi nd new posts every Welcome to Djibouti & Somaliland... 2 Somaliland, you’d be hard author-reviewed and recommended 12 seconds. Ethiopia, pressed to find a better Djibouti & combination of nature accommodation for any price range. Map .................................. 4 Somaliland and culture. The best part is, there’ll be no crowds to 17 Top Experiences ........ 6 hinder the experience. Book activities Discover and book amazing experiences Need to Know ................. 14 online for destinations around the globe. If You Like... ..................... 16 Month by Month ............. 19 lonelyplanet.com/destinations lonelyplanet.com/thorntreeonelyplanet.com/t A Land-lover’s Dream 13 Outdoor Adventures 15 Ethiopia’s landscape impresses in both 16 These countries beg outdoor escapade JOHN ELK/GETTY IMAGES © IMAGES ELK/GETTY JOHN scale and beauty. Travellers are thrilled by © CARILLET JEAN-BERNARD with their larger-than-life, hallucina- the amazing backdrop of canyons, chasms, tory landscapes.
    [Show full text]